This file was created by the TYPO3 extension publications --- Timezone: CEST Creation date: 2026-04-29 Creation time: 09:13:14 --- Number of references 19 article Schuster2025 Article 2025 10.1111/bor.70023 Boreas https://www.scopus.com/inward/record.uri?eid=2-s2.0-105009861202&doi=10.1111%2fbor.70023&partnerID=40&md5=e90b14fc9ce9aa2bf751e4ac310b3135 Cited by: 0; All Open Access, Hybrid Gold Open Access Bennet Schuster David Mair Timothy C. Schmid Lukas Gegg Marius W. Buechi Sebastian Schaller Flavio S. Anselmetti Frank Preusser article Furlanetto2025 Article 2025 10.1016/j.ancene.2025.100478 Anthropocene 51 https://www.scopus.com/inward/record.uri?eid=2-s2.0-105007879288&doi=10.1016%2fj.ancene.2025.100478&partnerID=40&md5=cee514018025b4a90fdb5984a229900a Cited by: 0 Giulia Furlanetto Renata Perego Marco Stefano Caccianiga Roberto Comolli Laura Ferigato Giulia Frigerio Cesare Ravazzi article Beraus20251587 Article 2025 10.1111/1365-2478.70024 Geophysical Prospecting 73 1587 – 1605 5 https://www.scopus.com/inward/record.uri?eid=2-s2.0-105003709148&doi=10.1111%2f1365-2478.70024&partnerID=40&md5=60aee09dd0466db30d2236861c2738a5 Cited by: 0 Sarah Beraus Daniel Köhn Thomas Bohlen Thomas Burschil Bennet Schuster Hermann Buness Gerald Gabriel article Burschil20251493 Article 2025 10.5194/se-16-1493-2025 Solid Earth 16 1493 – 1507 12 https://www.scopus.com/inward/record.uri?eid=2-s2.0-105024757270&doi=10.5194%2fse-16-1493-2025&partnerID=40&md5=c5bb77e0f56a7259ec6ba919e49b53d3 Cited by: 0; All Open Access, Gold Open Access, Green Open Access Thomas Burschil Daniel Köhn Matthias Körbe Gerald Gabriel Johannes Großmann Gustav Firla Markus Fiebig article Schaller2025 Article 2025 10.1186/s00015-025-00481-y Swiss Journal of Geosciences 118 1 https://www.scopus.com/inward/record.uri?eid=2-s2.0-105008513970&doi=10.1186%2fs00015-025-00481-y&partnerID=40&md5=906b427b6f1c809601e74fbb4c117dc2 Cited by: 0 Sebastian Schaller Bennet Schuster Sarah Beraus Marius W. Buechi Hermann Buness Flavio S. Anselmetti article Beraus2024237 Article 2024 10.5194/sd-33-237-2024 Scientific Drilling 33 237 – 248 2 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85206495700&doi=10.5194%2fsd-33-237-2024&partnerID=40&md5=1b6f9240b1b2bafa9e1a50b90df32fc8 Cited by: 0 Sarah Beraus Thomas Burschil Hermann Buness Daniel Köhn Thomas Bohlen Gerald Gabriel article Firla2024 Overdeepened valleys are structures scoured into the underlying substrate by glaciers that have been subsequently filled with sediment, which recorded the environmental history of the adjacent landscape. Investigated here is an overdeepened structure that was formed beneath the Salzach Paleoglacier west of Freilassing, Bavaria (southern Germany). In a previous study, infinite infrared stimulated luminescence (IRSL) ages have been determined for the lower part of the core using a multi-grain approach. Applying single-grain feldspar luminescence dating allows to identify the unsaturated signals, previously masked by multi-grain signal averaging. Identification of the normally distributed leading edge in equivalent dose (De) distributions allows for the dismissal of low value De (LOVED) grains that appear to reflect underestimating outliers. Measurement of eleven samples distributed along the entire length of the core yielded two distinct age clusters, for which fading corrected IRSL50 and uncorrected pIRIR225 ages agree within uncertainties. Whereas the younger age cluster at the top of the sequence is attributed to Marine Isotope Stage (MIS) 3, the older age cluster is assigned to MIS 6. It is shown that single grain pIRIR measurements will allow to resolve the infill chronology of overdeepened structures in the Alps, at least for the last ca. 200 ka. Overall, the present study represents a further step towards understanding and handling complex De distributions often encountered in single grain feldspar luminescence dating. This contributes to better understand the frequently observed age offset between single grain and single-aliquot measurements. © 2024 The Authors Article 2024 10.1016/j.quageo.2024.101627 Quaternary Geochronology 85 Elsevier B.V. https://www.scopus.com/inward/record.uri?eid=2-s2.0-85205438388&doi=10.1016%2fj.quageo.2024.101627&partnerID=40&md5=c1865dfe53cad1339c1a660a57b57f25 Cited by: 0; All Open Access, Hybrid Gold Open Access Gustav Firla Christopher Lüthgens Stephanie Neuhuber Clemens Schmalfuss Ernst Kroemer Frank Preusser Markus Fiebig article Schuster2024191 Article 2024 10.5194/sd-33-191-2024 Scientific Drilling 33 191 – 206 2 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85197588168&doi=10.5194%2fsd-33-191-2024&partnerID=40&md5=19c59c48d224db0569eff0363c74d069 Cited by: 9; All Open Access, Gold Open Access, Green Open Access Bennet Schuster Lukas Gegg Sebastian Schaller Marius W. Buechi David C. Tanner Ulrike Wielandt-Schuster Flavio S. Anselmetti Frank Preusser article Buechi2024 Article 2024 10.1016/j.quascirev.2024.108970 Quaternary Science Reviews 344 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85205137314&doi=10.1016%2fj.quascirev.2024.108970&partnerID=40&md5=5b060323e5498409c4e14bf654096184 Cited by: 0; All Open Access, Hybrid Gold Open Access Marius W. Buechi Angela Landgraf Herfried Madritsch Daniela Mueller Maria Knipping Franziska Nyffenegger Frank Preusser Sebastian Schaller Michael Schnellmann Gaudenz Deplazes article sd-32-27-2023 2023 10.5194/sd-32-27-2023 Scientific Drilling 32 27-42 S. Schaller M. W. Buechi B. Schuster F. S. Anselmetti article Buness2022 Article 2022 10.1016/j.jappgeo.2022.104614 Journal of Applied Geophysics 200 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85126938106&doi=10.1016%2fj.jappgeo.2022.104614&partnerID=40&md5=d5ca25b176e80043e1fd0ed06efb68bb Cited by: 3; All Open Access, Hybrid Gold Open Access Hermann Buness David Colin Tanner Thomas Burschil Gerald Gabriel Ulrike Wielandt-Schuster inproceedings anselmetti2022drilling 2022 EGU General Assembly Conference Abstracts EGU22--3165 Flavio Anselmetti Marius Buechi article Anselmetti202251 The sedimentary infill of glacially overdeepened valleys (i.e., structures eroded below the fluvial base level) is an excellent but yet underexplored archive with regard to the age, extent, and nature of past glaciations. The ICDP project DOVE (Drilling Overdeepened Alpine Valleys) Phase 1 investigates a series of drill cores from glacially overdeepened troughs at several locations along the northern front of the Alps. All sites will be investigated with regard to several aspects of environmental dynamics during the Quaternary, with focus on the glaciation, vegetation, and landscape history. Geophysical methods (e.g., seismic surveys), for example, will explore the geometry of overdeepened structures to better understand the process of overdeepening. Sedimentological analyses combined with downhole logging, analysis of biological remains, and state-of-the-art geochronological methods, will enable us to reconstruct the erosion and sedimentation history of the overdeepened troughs. This approach is expected to yield significant novel data quantifying the extent and timing of Middle and Late Pleistocene glaciations of the Alps. In a first phase, two sites were drilled in late 2021 into filled overdeepenings below the paleolobe of the Rhine Glacier, and both recovered a trough filling composed of multiphase glacial sequences. Fully cored Hole 5068_1_C reached a depth of 165m and recovered 10m molasse bedrock at the base. This hole will be used together with two flush holes (5068_1_A, 5068_1_B) for further geophysical cross-well experiments. Site 5068_2 reached a depth of 255m and bottomed out near the soft rock-bedrock contact. These two sites are complemented by three legacy drill sites that previously recovered filled overdeepenings below the more eastern Alpine Isar-Loisach, Salzach, and Traun paleoglacier lobes (5068_3, 5068_4, 5068_5). All analysis and interpretations of this DOVE Phase 1 will eventually lay the ground for an upcoming Phase 2 that will complete the pan-Alpine approach. This follow-up phase will investigate overdeepenings formerly occupied by paleoglacier lobes from the western and southern Alpine margins through drilling sites in France, Italy, and Slovenia. Available geological information and infrastructure make the Alps an ideal area to study overdeepened structures; however, the expected results of this study will not be restricted to the Alps. Such features are also known from other formerly glaciated mountain ranges, which are less studied than the Alps and more problematic with regards to drilling logistics. The results of this study will serve as textbook concepts to understand a full range of geological processes relevant to formerly glaciated areas all over our planet. © Copyright: 2022 English 18168957 10.5194/sd-31-51-2022 Scientific Drilling 31 Copernicus Publications 51-70 Institute of Geological Sciences, Oeschger Centre for Climate Change Research, University of Bern, Bern, 3012, Switzerland; Geological Survey of Slovenia, Ljubljana, 1000, Slovenia; Department of Geology, Université Savoie Mont Blanc, Université Grenoble Alpes, CNRS, IRD, ISTerre, Chambéry, France; Department of Civil Engineering and Natural Hazards, Institute of Applied Geology, University of Natural Resources and Life Sciences, Vienna (BOKU), Vienna, 1190, Austria; Department 1: Seismics, Gravimetry & Magnetics, Leibniz Institute for Applied Geophysics, Hanover, 30655, Germany; Institute of Geology, Leibniz University Hanover, Hanover, 30167, Germany; Institute of Earth and Environmental Sciences, University of Freiburg, Freiburg, 79104, Germany; CNR - Institute of Environmental Geology and Geoengineering (IGAG), Milan, 20126, Italy; Univ. of Geneva, Geneva, Switzerland; LIAG Hanover, Hanover, Germany; Univ. Hanover, Hanover, Germany; Univ. Bern, Bern, Switzerland; LIAG, Hanover, Germany; BGR Hanover, Hanover, Germany; ENSI, Brugg, Switzerland; Nagra, Wettingen, Switzerland; GBA, Vienna, Austria; BOKU Vienna, Vienna, Austria; Univ. Freiburg, Freiburg, Germany; Dr. von Moos AG, Gächlingen, Switzerland; ICDP-OSG, Potsdam, Germany; Eawag, Dübendorf, Switzerland; LfU, Augsburg, Germany; CNR-IGG, Padova, Italy; CNR-IGAG, Milan, Italy; Univ. Salzburg, Salzburg, Austria; ETH Zürich, Zürich, Switzerland; Univ. Leoben, Leoben, Austria; Univ. Illinois, Champaign, United States; Univ. Geneva, Geneva, Switzerland; LGRB, Freiburg, Germany Core drilling; Drills; Environmental impact; Geochronology; Glacial geology; Infill drilling; Landforms, Alpine valleys; Downholes; Drill core; Environmental dynamics; Fluvials; Geophysical methods; Phase 1; Sedimentary infill; Sedimentological analysis; Seismic surveys, Recovery https://www.scopus.com/inward/record.uri?eid=2-s2.0-85141937567&doi=10.5194%2fsd-31-51-2022&partnerID=40&md5=584a0194d41bc87e376fcf3a5277c0c2 cited By 0 F.S. Anselmetti M. Bavec C. Crouzet M. Fiebig G. Gabriel F. Preusser C. Ravazzi D. Ariztegui S. Beraus A.-C. Brandt M. Buechi H. Buness T. Burschil G. Deplazes G. Götzl G. Firla L. Gegg H.R. Graf K. Heeschen R. Kipfer E. Kroemer C. Lüthgens G. Monegato S. Neuhuber R. Pini J. Reitner B. Salcher S. Schaller C. Schmalfuss C. Schmelzbach R. Scholger B. Schuster A. Stumpf D.C. Tanner C. Thomas Y. Tomonaga U. Wieland-Schuster T. Wonik Dove Scientific Team article burschil2022near 2022 Near Surface Geophysics 20 Wiley Online Library 331--348 4 Thomas Burschil Hermann Buness Cedric Schmelzbach inproceedings brandt2021shape 2021 EGU General Assembly Conference Abstracts EGU21--5996 Anna-Catharina Brandt David C Tanner Hermann Buness Thomas Burschil Gerald Gabriel article Burschil2018593 Article 2018 10.1002/nsg.12011 Near Surface Geophysics 16 593 – 610 6 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85062991714&doi=10.1002%2fnsg.12011&partnerID=40&md5=9f6efc56e3dcb74ba36d92c5783ea640 Cited by: 21; All Open Access, Hybrid Gold Open Access Thomas Burschil Hermann Buness David C. Tanner Ulrike Wielandt-Schuster Dietrich Ellwanger Gerald Gabriel conference Burschil2017 A high-resolution P-wave vibroseis reflection survey and PSDM processing are used to image the structure of the Tannwald Basin, a 250 m-deep, distal branch basin of the Rhine Glacier. The basin substratum, the basin base, as well as the basin infill could be identified. The subglacial deposits (e.g. till) can be clearly distinguished from basin fines (e.g. marl, silt and sand). We identified five seismic facies as well as a number of subfacies. Internal features of the basin comprises an allochthonous Molasse block and a system of eskers in section. The interpretation will be used to locate a drill site for the ICDP-project DOVE and provides information for S-wave and multi-component processing. 2017 English 9789462822238 10.3997/2214-4609.201702101 23rd European Meeting of Environmental and Engineering Geophysics European Association of Geoscientists and Engineers, EAGE Liang, Sweden Fertilizers; Seismic waves; Seismology; Shear waves, Drill sites; High resolution; Internal features; Multicomponents; P waves; S-waves; Seismic facies; Vibroseis, Infill drilling https://www.scopus.com/inward/record.uri?eid=2-s2.0-85088410688&doi=10.3997%2f2214-4609.201702101&partnerID=40&md5=d36c6b840f371c0a6cfbfbb257a5e460 cited By 2 T. Burschil H. Buness D. Tanner G. Gabriel C. Krawczyk conference Buness2016 Overdeepened valleys and basin can be found in glaciated regions worldwide. Due to their geological, ecological, and societal relevance they constitute a relevant geoscientific target. In preparation for an ICDP project (Drilling Overdeepened Alpine Valleys, DOVE), we carried out several reflection seismic surveys using high-resolution P-wave, horizontally pola¬ri¬zed SH-wave, and multi-component (SV-And SH-wave sources, 3-component re¬ceiver) techniques at a test site in the Tannwald basin north of Lake Constance. The first results of the P-And SH-wave reflection profiles are presented here. The seismic sections image well the internal valley structure of the Tannwald Basin; different facies are also distinguishable in the glacial sediments. The combined inter¬pretation of P-wave and SH-wave reflection seismics reveal more details than just one technique on its own by providing complementary information. P-wave seismics show a more coherent image with a higher penetration depth, while SHwave seismics partly resolve more details due to their higher resolution. The combination promises to be an enhanced tool to investigate sedimentary successions in advance of scientific drilling. 2016 English 22nd European Meeting of Environmental and Engineering Geophysics, Near Surface Geoscience 2016 European Association of Geoscientists and Engineers, EAGE Leibniz Institute for Applied Geophysics (LIAG), Germany Geology; Geophysics; Landforms; Seismic waves; Seismology, Coherent images; Glacial sediments; High resolution; Higher resolution; Multicomponents; Reflection seismic; Scientific drilling; Seismic sections, Shear waves https://www.scopus.com/inward/record.uri?eid=2-s2.0-85007363519&partnerID=40&md5=e314ca6b510deb4b69c0bd8b9d885383 cited By 0 H. Buness T. Burschil G. Gabriel article pini2013report 2013 Alpine and Mediterranean Quaternary 26 vii--ix 1 Roberta Pini